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Rocks & Minerals Eng
| Term | Definition |
|---|---|
| Minerals are ... | Solid, inorganic, naturally occurring, definite atomic structure and composition, homogenous (same) |
| Properties of Minerals | Color, streak, hardness, luster, cleavage/fracture, specific gravity/density |
| Properties of Minerals - Color | Visual color, not very reliable |
| Properties of Minerals - Streak | Color in powdered form, more reliable |
| Properties of Minerals - Hardness | Mineral's resistance to being scratched |
| Moh's Scale | Measures mineral hardness |
| Softest mineral on Moh's Scale | Talc |
| Hardest mineral on Moh's Scale | Diamond |
| Luster | Metallic or non-metallic |
| Cleavage | Mineral breaking along an even plane |
| Fracture | Uneven breaking (like how glass breaks) |
| Specific gravity | Mineral density |
| Rocks are ... | Made of minerals |
| Criteria for classifying rocks | Formed from one or more minerals, solid, formed in nature, can be organic or inorganic |
| Three rock types | Sedimentary, igneous, metamorphic |
| Rock type depends on | How they're formed, texture, and composition |
| Igneous rocks are formed by | cooling and solidification of maga/lava |
| Igneous rocks can be formed in two places - | intrusive and extrusive |
| Intrusive | Formed inside the Earth's crust, cools slowly, large crystals, from magma |
| Extrusive | Formed outside the Earth's crust/on the surface, cools quickly, small crystals, from lava, can be glassy or vesicular |
| Sedimentary rocks are formed by | weathering, erosion, deposition, burial, compaction, and cementation |
| Three types of sedimentary rocks | Clastic, chemical, bioclastic |
| Clastic rocks | visible pieces of rock, jagged or smooth |
| Chemical Rocks | formed from dissolved minerals in water |
| Bioclastic rocks | Formed from shells and other organic matter |
| Fossils can be found in what type of rock? | Sedimentary |
| Metamorphic Rocks | Formed under heat and pressure (no melting) of other rocks |
| Metamorphic characteristics | Realignment of minerals, ex. layering and folding |
| Two metamorphism types | Regional and Contact |
| Regional metamorphism | Over large surfaces, caused by big events like orogenies (mountain building) or plates colliding - high pressure |
| Contact metamorphism | Lava or magma comes into contact with rock, intense heat causes metamorphosis |